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RAREX LIMITED Capital/Financing Update 2017

Nov 30, 2017

65681_rns_2017-11-30_42f1bfa6-a268-4b51-8e0d-26d5f94960d1.pdf

Capital/Financing Update

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Clancy Exploration Limited Phone:(08) 6143 6720
Suite 23, 513 Hay Street
Subiaco WA 6008 www.clancyexploration.com
Australia [email protected]
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ASX / MEDIA ANNOUNCEMENT 01 December 2017

Acquisition of Highly Prospective Pilbara Gold Project

  • Clancy to acquire Hong Kong Gold Project in highly prospective Pilbara region.

  • Granted licence tenure of 40km[2] with a prospective strike length of over 5km.

  • Mapping outlines presence of highly prospective lower Fortescue Group lithologies.

  • Lithologies recently identified by Novo Resources (TSX-V: NVO) as “the key stratigraphy to the recent new conglomerate gold discoveries within the region”

  • Project includes historical eluvial and alluvial gold mines located at Hong Kong Far West, Empress North and John Bull West.

  • Better high grade rock chip samples across project tenure include:

  • 71.4g/t Au from John Bull Prospect

  • 45.5g/t Au & 6.9g/t Au from Last Chance Prospect

  • 33.2g/t Au from Princess May South Prospect

  • 14.9g/t Au from Foochow Prospect

  • 5.4g/t Au from Hong Kong Prospect

  • Exploration program to commence immediately, subject to clearance from native title parties.

Clancy Exploration Limited (ASX: CLY) is pleased to announce that it has reached an agreement to acquire the Hong Kong Gold Project (the “Project” ) located in the Pilbara region of Western Australia (Figure 1).

The project contains over five strike kilometres of lower Fortescue Group rocks including both the Hardey Formation and the Mount Roe Basalt, as mapped by the Geological Survey of Western Australia (GSWA). Novo Resources describe this stratigraphy as being “the key to the recent new conglomerate gold discoveries in the region”.

Previous explorers have also targeted Archaean lode hosted gold mineralisation and VMS mineralisation.

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Clancy Exploration Limited (ASX: CLY)

ASX / Media Announcement

Figure 1: Location of Hong Kong Tenement – Western Pilbara

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Location, Infrastructure & Tenure:

The Project is located 100km south-southwest of Port Hedland in the Western Pilbara Goldfield of Western Australia. Access to the Project is via the sealed Great Northern Highway for 100km south of Port Hedland thence via good quality graded roads.

The Hong Kong Gold Project consists of a single Exploration Licence, 47/3566, covering 40km[2] with an expiry date of 19 July 2022.

The exploration licence is located wholly within the Yandeyarra Aboriginal Reserve.

Project Geology:

GSWA mapping has outlined a highly prospective >5km strike length of the basal contact between the Mt Roe Basalt and older Archaean Basalt.

The Mt Roe Basalt forms as distinctive red ridges with well-developed scree slopes. The Hardey Formation essentially comprises of conglomerate with a few minor interbedded sandstone occurrences. The polymictic conglomerate includes clasts

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Clancy Exploration Limited (ASX: CLY)

ASX / Media Announcement

of basalt, chert, granite, shale, dolerite and other lithologies with diameters up to 1m. The clasts are rounded to angular.

Numerous prospecting workings (dryblowing) were located along creeks draining from the conglomerate.

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Figure 2: Hong Kong Project- Geology & Occurrences

The Archaean Pilbara Well Greenstone belt crops out southeast of the Lower Fortescue Group lithologies. The greenstone belt includes metabasalts, ultramafics and silicified sediments which have been metamorphosed and deformed by up to three phases of ductile deformation.

Historical Exploration & Mining:

John Bull

The John Bull workings have collapsed obscuring the scale of the historical operations. A tight, sub-vertical fault with quartz veins that strike 025[o] lies exposed in a 40m deep shaft developed in carbonated mafic rock at the main cluster of workings. Mullock includes minor quartz-carbonate vein material. Quartz porphyry occurs immediately west of the main workings.

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Clancy Exploration Limited (ASX: CLY)

ASX / Media Announcement

A shallow pit sunk into fresh metabasalt, 100m east of the main workings, has exposed deformed quartz-carbonate-chlorite veins with apple green sericite and disseminated native gold. Rock chip sampling of the quartz-carbonate veining has reported up to 71.4g/t gold.

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Figure 3: Regional Geology & Mineral Occurrences

Last Chance

Last Chance workings comprise of a 4m deep stope extending for 20m on a 20cm wide quartz-carbonate vein. Chip samples from laminated quartz veins reported results of up to 45.5 g/t gold.

Princess May

Historical workings extend over 150m strike length. A tight fault with quartz veins striking 015 to 025[o] and dipping 65-70[o] East, is exposed in several shafts and stopes

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Clancy Exploration Limited (ASX: CLY)

ASX / Media Announcement

developed to a maximum depth of 40m. Mullock samples include variably altered chlorite-carbonate-sericite mafic rock. Laminated quartz-carbonate veining contains limonite pseudomorphs (after sulphide) and lamellae of apple-green sericite. Sampling of the quartz-carbonate vein material reported up to 33.2 g/t gold.

Foochow

Foochow is a series of pits and stopes that extend over a strike of 70m, to around 10m depth. Mullock dumps carry chlorite-carbonate-sericite altered dolerite commonly with limonite pseudomorphs. A single rock chip sample taken of laminated quartz vein material reported 14.9 g/t gold.

Empress

Empress workings comprise of a deep shaft to approximately 40m and stoping has occurred over 50m strike length. Mullock material surrounding the shaft is massive to weakly foliated dolerite, variably altered to chlorite-carbonate-sericite. Numerous small quartz-carbonate-pyrite veins cut the altered dolerite. Sampling of laminated quartz vein material, north of the workings, reported 11.2 g/t gold.

Hong Kong

Hong Kong is represented by a group of workings comprising of a 20m shaft and two stopes of similar depth located over northeast-striking structures developed in altered mafic rock, including dolerite. More workings extend 160m north-northeast of Hong Kong where a 10m deep shaft and stopes extend over 40 metres of strike.

Mullock dumps indicate extensive chlorite-carbonate alteration of mafic host rocks and laminated quartz-carbonate veins. More intense alteration in narrow proximal zones (adjacent to veins) comprise of bleached zones of sericite and carbonate. Sampling of quartz vein material reported results of up to 5.35 g/t Au.

Empress East #2

A 40m long series of stopes and pits. The deepest extent of workings is approximately 10m. Mullock is massive but strongly carbonated mafic lithologies with small quartzcarbonate veining and apple green sericite on vein margins. Altered wall rock sample reported 0.054 g/t Au.

Arizona

Arizona is located a few hundred metres east of the Princess May workings. The strong carbonate alteration evident suggests that Arizona lies within the John Bull Shear Zone. Sampling conducted across a variety of styles of alteration and mineralisation reported values up to 1.24 g/t gold in a quartz-chlorite porphyry. The porphyry is similar to that observed at John Bull.

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Clancy Exploration Limited (ASX: CLY)

ASX / Media Announcement

Commercial Terms

Clancy Exploration Ltd has reached agreement to acquire 100% of the Hong Kong Project from Red Field Pty Ltd via the issue of 270,000,000 fully paid ordinary shares at an issue price of $0.005 per share, for a total value of $1.35 million. The issue of the consideration shares falls within Clancy’s existing ASX Listing Rule 7.1 placement capacity.

Competent Persons Statement:

The information in this announcement that relates to the Exploration Results for Hong Kong Gold Project is based on information compiled and fairly represented by Mr Jonathan King, who is a Member of the Australian Institute of Geoscientists and Consultant to Clancy Exploration Ltd. Mr King has sufficient experience relevant to the style of mineralisation and type of deposit under consideration, and to the activity which he has undertaken, to qualify as a Competent Person as defined in the 2012 Edition of the Joint Ore Reserves Committee (JORC) Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves. Mr King consents to the inclusion in this report of the matters based on this information in the form and context in which it appears.

Please direct enquiries to: Scott Patrizi Phone: +61 8 6143 6720 Email: [email protected] Web: www.clancyexploration.com

Disclaimer:

Forward-looking statements are statements that are not historical facts. Words such as “expect(s)”, “feel(s)”, “believe(s)”, “will”, “may”, “anticipate(s)” and similar expressions are intended to identify forward-looking statements. These statements include, but are not limited to statements regarding future production, resources or reserves and exploration results. All of such statements are subject to certain risks and uncertainties, many of which are difficult to predict and generally beyond the control of the Company, that could cause actual results to differ materially from those expressed in, or implied or projected by, the forward-looking information and statements. These risks and uncertainties include, but are not limited to: (i) those relating to the interpretation of drill results, the geology, grade and continuity of mineral deposits and conclusions of economic evaluations, (ii) risks relating to possible variations in reserves, grade, planned mining dilution and ore loss, or recovery rates and changes in project parameters as plans continue to be refined, (iii) the potential for delays in exploration or development activities or the completion of feasibility studies, (iv) risks related to commodity price and foreign exchange rate fluctuations, (v) risks related to failure to obtain adequate financing on a timely basis and on acceptable terms or delays in obtaining governmental approvals or in the completion of development or construction activities, and (vi) other risks and uncertainties related to the Company’s prospects, properties and business strategy. Our audience is cautioned not to place undue reliance on these forward-looking statements that speak only as of the date hereof, and we do not undertake any obligation to revise and disseminate forward-looking statements to reflect events or circumstances after the date hereof, or to reflect the occurrence of or non-occurrence of any events

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Clancy Exploration Limited (ASX: CLY)

ASX / Media Announcement

APPENDIX 1: Rock Chip Sampling Results

Sample Easting North Prospect **Auppm ** Description
55121 637,233 7,657,911 Arizona 0.06 Chertpyriticquartz vein
55122 637,209 7,657,920 Arizona 0.015 Chert with malachite stain
55123 637,214 7,657,494 Arizona 0.045 Pyriticquartzporphyry
55124 637,305 7,657,500 Arizona 0.011 Carbonated mafic
550076 637,779 7,657,651 Arizona 0.005 Quartz vein in carbonated basalt
550077 637,777 7,657,660 Arizona 0.889 Quartzporphyrywith coarsepyrite
550078 637,775 7,657,665 Arizona 0.22 Quartz vein in carbonated mafic
550079 637,780 7,657,692 Arizona 0.012 Carbonated and bleached mafic
550080 637,773 7,657,742 Arizona 0.075 Quartz porphyry with quartz stingers
and coarsepyrite. Sheared@040
550081 637,786 7,657,756 Arizona 0.008 Quartz vein with carb and chlorite
alteration from mafic from
550082 637,984 7,657,409 Arizona 0.422 Quartz vein with carbonate and
tourmaline
550083 637,748 7,657,748 Arizona 0.109 Weak quartz stringers in quartz porch
and weakpyrite
550084 637,974 7,657,382 Arizona 0.025 Carbonatedgreywacke
550085 637,961 7,657,382 Arizona 0.006 Quartz carbonate chlorite vein on
contact between greywacke and
basalt. Sheared@110o
550086 637,978 7,657,378 Arizona 0.014 Quartz carbonate vein in greywacke.
Quartz stringers normal to vein trend
@110o
550087 637,644 7,657,632 Arizona 0.072 Quartz stingers and quartz chlorite
vein inquartzporphyry
550088 637,644 7,657,627 Arizona 0.011 Quartz vein ingreywacke
550089 637,651 7,657,628 Arizona 0.015 Quartz‐carb vein ingreywacke
550090 637,590 7,657,599 Arizona 0.025 Pyritic aplite with fine grained
disseminated pyrite. Dark grey when
fresh. Strike 100o
550091 637,585 7,657,603 Arizona 0.145 Blue‐grey pyritic chert. Strike 100o
550092 637,589 7,657,614 Arizona 0.003 Quartz vein in greywacke. Foliation
100o
550093 637,588 7,657,550 Arizona 0.033 Pyritic blue‐grey chert. Strike 230o.
Dip32otowards NW
550094 637,604 7,657,544 Arizona 1.24 Quartz‐chlorite porphyry. Pyritic and
quartz veined. Strike 075o
550095 637,604 7,657,548 Arizona 0.107 Sheared basalt with quartz carbonate
veins. Foliation 095o
550096 637,416 7,657,137 Arizona 0.043 Quartzporphyrywithpinkquartz
550097 637,412 7,657,146 Arizona 0.009 Silicified and sheared greywacke with
minorquartz stingers

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Clancy Exploration Limited (ASX: CLY)

ASX / Media Announcement

Sample Easting North Prospect **Auppm ** Description
550098 637,405 7,657,155 Arizona 0.359 Quartz‐chlorite porphyry. Pyritic and
quartz veined.
550099 637,411 7,657,173 Arizona 0.33 Quartz‐feldspar porphyry with pyrite
andquartz veins
550100 637,389 7,657,150 Arizona 0.427 Quartz‐veinedgreywacke
550208 637,400 7,657,092 Arizona 0.006 Red pyritic and quartz veinlets in small
felsicporphyry
550209 637,399 7,657,091 Arizona 0.013 Qtz‐crb‐pyr veinlets in crb altered
sheared mafic
550210 637,386 7,657,086 Arizona 0.004 Vfg greyfelsic dyke
550211 637,361 7,657,101 Arizona 0.005 Qtz crb veinlets in sheared mafic‐ crb
altered
550212 637,346 7,657,096 Arizona 0.709 Red siliceous mafic with qtz veinlets
andpyr alteration
550213 637,348 7,657,165 Arizona 0.2 Red grey siliceous porphyry‐ fine
grained mafic porphs‐ crb‐pyrite
altered
550214 637,405 7,657,152 Arizona 0.006 Red grey siliceous felsic porph with
crb alt and tracepyr
550215 637,404 7,657,153 Arizona 0.026 Qtz crb veinlets in mafic along porph
(550214)contact
550216 637,422 7,657,154 Arizona 0.164 Lightgrey qtz felsicporph w trpyr
550217 637,436 7,657,163 Arizona 1.14 Light grey felsic qtz porph sl.
Weathered w 5%pyrpseudo's
550218 637,414 7,657,183 Arizona 0.153 Red grey siliceous and crb alt porph w
trpyr on hill
550219 637,444 7,657,273 Arizona 0.07 Light grey qtz feldspar porph w pyr
pseudo's 1% and traceqtz veinlets
550220 637,423 7,657,304 Arizona 0.958 Red dk grey fractured porph with
mafic crysts‐ silca crb alt‐ tr pyr
pseudo's and 10%qtz veinlets
550221 637,412 7,657,323 Arizona 0.554 Veining and silca crb alt country rock
on nth side of slope
550222 637,499 7,657,352 Arizona 0.616 Dk grey red fractured siliceous porph
finegrained
550223 637,497 7,657,352 Arizona 0.074 Country rock with qtz crb veins on
contact with 550222
550224 637,509 7,657,344 Arizona 0.128 Lightgrey qtz feldsporph‐ trpyr
550225 637,528 7,657,308 Arizona 0.007 Dk grey siliceous vfg with fg fresh pyr
(trace)mafic crysts dyke
550226 637,465 7,657,191 Arizona 0.227 Lightgrey qtz feldsparporph
550305 637,729 7,657,343 Arizona 0.017 Strongly carbonate altered basalt with
quartz carbonate veins
550401 636,998 7,656,601 Arizona 0.262 Quartz porphyry with quartz stringers.
Minorpyrite. Strike 050

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Clancy Exploration Limited (ASX: CLY)

ASX / Media Announcement

Sample Easting North Prospect **Auppm ** Description
550402 637,014 7,656,568 Arizona 0.01 Pyritic greywacke. Minor pyrite.
Chlorite and carbonate alteration.
550403 636,938 7,656,566 Arizona 0.275 Quartzporphyrywithquartz veins
550404 636,943 7,656562 Arizona 0.015 Weakly quartz veined basalt. Some
quartz carbonate veining
550405 636,907 7,656473 Arizona 0.024 Quartz‐tourmaline vein along fault in
carbonate altered greywacke. Dip 27‐
Strike 056o
550406 636,891 7,656453 Arizona 1.21 Quartz vein in carbonatedgreywacke
550407 636,897 7,656503 Arizona 0.237 Quartz‐porphyrywithquartz stringers
550408 636,811 7,655938 Arizona 0.2 Quartz‐feldspar porphyry with quartz
veins and minorpyrite
550409 636,815 7,655926 Arizona 0.24 Pyritic blue‐greychert.
550410 636,771 7,655947 Arizona 0.18 Pyriticquartz‐feldsparporphyry
550411 636,800 7,655993 Arizona 0.082 Carbonated sediments (greywacke)
with carbonate veining
550412 636,805 7,655980 Arizona 0.032 Sheared chloriticgreywacke
550413 636,856 7,656125 Arizona 0.002 Quartz and fuchsite altered felsic rock
with quartz stingers and minor
carbonate alteration.
550414 636,843 7,656140 Arizona 0.003 Quartz and fuchsite altered felsic rock
withquartz vein
550415 636,841 7,656147 Arizona 0.003 Quartz‐carb veined basalt
550416 636,825 7,656150 Arizona 0.007 Quartz and fuchsite altered felsic rock
withquartz vein
550417 636,812 7,656159 Arizona 0.001 Sheared mafic with quartz vein and
carb and fuchsite alteration
550418 637,207 7,655997 Arizona 0.002 Silicified and carbonated felsic
intrusive
550419 637,201 7,656036 Arizona 0.009 Silicified and ferruginised mafic
550420 637,392 7,656504 Arizona 0.464 Quartz‐carb veined mafic with quartz‐
tourmaline veins
550421 637,384 7,656521 Arizona 0.01 Quartz porphyry with quartz‐
tourmaline veins andquartz stringers
550422 637,726 7,656735 Arizona 0.002 Silicified and quartz veined zone next
to sheared mafic
550423 637,732 7,656736 Arizona 0.001 Sheared basalt. Carbonated. Foliation
090o
550424 637,725 7,656743 Arizona 0.002 Silicified basalt with minorpyrite
550425 638,329 7,657227 Arizona 0.003 Basalt with minorquartz vein
550426 638,320 7,657222 Arizona 0.002 Quartz‐feldsparporphyry
550427 638,347 7,657230 Arizona 0.004 Quartz veinedgreywacke
550428 638,369 7,657241 Arizona 0.004 Quartz‐feldspar porphyry with chlorite
alteration
55113 633,915 7,658078 Empress 0.038 Altered dolerite

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Clancy Exploration Limited (ASX: CLY)

ASX / Media Announcement

Sample Easting North Prospect **Auppm ** Description
55112 634,457 7,657997 Empress
East
0.054 Carbonated mafic + veins
55118 631,594 7,655,955 Empress
Well
North
11.2 Laminated quartz vein
55119 631,627 7,655,972 Empress
Well
North
0.099 Choratised basalt
55120 631,627 7,655,972 Empress
Well
North
9.54 Laminated quartz sulphide vein
55111 634,336 7,657,211 Foochow 14.9 Laminatedquartz vein
55105 633,573 7,656,461 Hong
Kong
0.958 Laminated quartz vein
55106 633,573 7,656,461 Hong
Kong
0.058 Serecite carbonate alteration
55107 633,553 7,656,464 Hong
Kong
5.35 Quartz vein
55051 635,758 7,655,283 John Bull 0.134 Quartzporphyrywithpyrite
55052 635,617 7,655,024 John Bull 0.007 Carbonated mafic
55053 635,616 7,655,006 John Bull 71.4 Quartz carbonate vein
55054 635,716 7,654,970 John Bull 10.1 Mafic rock withQuartz chlorite veins
550235 635,208 7,654,530 John Bull 0.233 Small qtz veinlets in light grey qtz
feldsparporph
550236 635,246 7,654,535 John Bull 0.015 Whiteqtz vein
550237 635,259 7,654,546 John Bull 0.039 Light grey white qtz vein with fresh
and tarnishedpyr
550238 635,262 7,654,545 John Bull 0.174 Porphyry‐ light grey with trace pyrite
(mainlyon surfaces)andqtz veins
550239 635,236 7,654,503 John Bull 0.062 Qtz breccia veining in light grey felsic
porphyry
550240 635,100 7,654,387 John Bull 0.004 Whiteqtz vein
550241 635,169 7,654,465 John Bull 2.72 White qtz vein in strongly crb altered
mafic
550242 635,134 7,654,508 John Bull 0.317 Pyritic (tarnishing) white qtz vein and
yellow sulphates
550314 635,529 7,655,033 John Bull 0.007 Fine grained quartz porphyry with
minor ex‐pyrite
550315 635,542 7,655,059 John Bull 0.016 Fine grained blue‐grey quartz
porphyry
550316 635,607 7,655,099 John Bull 0.027 White coarse grained porphyry with
ex‐pyrite. Highlyweathered
550317 635,622 7,655,110 John Bull 0.032 Fine grained highly siliceous blue‐grey
porphyry. Possibly a few ex‐pyrite
holes.
550318 635,642 7,655,138 John Bull 0.154 Quartz vein in finegrainedporphyry

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Sample Easting North Prospect **Auppm ** Description
550319 635,665 7,655,165 John Bull 0.164 Whiteporphyrywith minor ex‐pyrite
550320 635,685 7,655171 John Bull 0.035 Fine grained porphyry with dark cubes
‐ sulphides or carbonate. Highly
weathered.
550321 635,708 7,655182 John Bull 0.052 Fine grained quartz porphyry with
pale green colour (sericite alteration)
and fine disseminatedpyrite
550322 635,722 7,655202 John Bull 0.012 Dark purple zone within blue‐grey
porphyry. Veryfinegrained.
550323 635,731 7,655219 John Bull 0.002 Dark purple zone in grey‐blue
porphyry. Fine grained with 2mm
quartz eyes.
550324 635,741 7,655250 John Bull 0.012 Dark purple fine grained zone with up
to 2mmquartz eyes.
550325 635,756 7,655277 John Bull 0.003 Blue grey porphyry on western edge
of outcrop.
550326 635,769 7,655306 John Bull 0.024 Coarse grained. Grey‐blue porphyry
with ex‐pyrite.
550327 635,773 7,655328 John Bull ‐0.001 Coarsegrained mafic rock.
550328 635,772 7,655325 John Bull 0.014 Fine grained sediment approx. 70cm
thick between mafic andporphyry.
550329 635,769 7,655327 John Bull 0.019 Felsic porphyry with fine grained and
disseminatedpyrite.
550330 635,794 7,655343 John Bull 0.039 Whiteporphyrywith minor ex‐pyrite
550331 635,817 7,655392 John Bull 0.008 Quartz‐feldspar porphyry. Dark purple
when fresh.
550332 635,805 7,655400 John Bull 0.104 Quartzporphyry
550333 635,808 7,655391 John Bull 0.002 Fine grained mafic intrusion between
twoporphyryunits.
550334 635,811 7,655441 John Bull 0.033 Fine grained blue‐grey porphyry with
minor ex‐pyrite.
550335 635,864 7,655499 John Bull 0.074 Blue‐grey porphyrywith minorpyrite.
550336 635,738 7,655571 John Bull ‐0.001 Mafic with weak carbonate alteration
andquartz stringers
550337 635,820 7,655485 John Bull ‐0.001 Mafic to the west of the porphyry.
Finegrained and massive.
550338 635,969 7,655367 John Bull 0.007 Fine grained sediment with carbonate
stringers.
550339 635,992 7,655347 John Bull 0.003 Basalt with carbonate alteration and
carbonate veins with tremolite on
fractures.
550340 636,009 7,655405 John Bull 0.021 Sediment. Fine grained with minor
quartz and carbonate veins.
550341 636,013 7,655397 John Bull 0.005 Mafic with carbonate alteration and
minor ex‐pyrite.

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ASX / Media Announcement

Sample Easting North Prospect **Auppm ** Description
550342 635,989 7,655361 John Bull 0.002 Quartz‐chlorite vein on boundary
between sediments and carbonate
altered mafic.
550343 635,803 7,655,303 John Bull 0.024 Cross‐cutting quartz veins in fine
grained mafic sediment.
550344 635,471 7,654,968 John Bull 0.017 Whitequartzporphyry
550345 635,337 7,654,727 John Bull 0.059 Felsic volcanic ‐ fine grained‐ grey‐
blue colour.
550346 635,333 7,654,722 John Bull 0.032 Fine grained quartz porphyry with ex‐
pyrite.
550347 635,334 7,654,725 John Bull 0.006 Sediments (greywacke) adjacent to
felsics‐ with carbonate veining.
550348 635,233 7,654,648 John Bull 0.019 Fine grained quartz porphyry ‐ blue
greywith minorpyrite.
550349 635,111 7,654,636 John Bull 0.028 Quartzporphyrywith minor ex‐pyrite.
550350 635,010 7,654,586 John Bull 0.005 Felsic volcanic.
550351 634,764 7,654,163 John Bull 0.048 Mafic rock (basalt) with minor quartz
stringers andquartz vein.
550352 634,734 7,654,045 John Bull 0.013 Quartz‐feldsparporphyry.
550353 634,716 7,654,027 John Bull 0.005 Quartz vein in fine grained ultramafic
rock
550354 634,426 7,654,003 John Bull 0.003 Mafic rock.
550355 635,697 7,653,657 John Bull 0.015 Quartz porphyry with fine grained
disseminated ex‐pyrite and cross‐
cutting quartz veins.
550356 635,685 7,653,648 John Bull 0.001 Carbonate altered basalt.
550357 635,672 7,653,606 John Bull 0.004 Sediment (greywacke) with quartz
veins and carbonate veins.
550358 635,663 7,653,645 John Bull 0.008 White quartz porphyry with quartz
stringers and minor ex‐pyrite.
550359 635,612 7,653,662 John Bull 4.2 Highly silicified rock ‐ possibly
originally sedimentary with quartz
vein.
550360 636,165 7,655,916 John Bull 0.029 Darkpurplequartzporphyry
550361 636,162 7,655,947 John Bull 0.016 Quartz porphyry with minor
disseminated ex‐pyrite.
55108 633,635 7,656,582 Last
Chance
6.93 Quartz veining + proximised wall rock
55109 633,648 7,656,602 Last
Chance
45.5 Laminated quartz vein
55110 633,802 7,656,779 Last
Chance
0.168 Strongly carbonated mafic rock
55048 636,710 7,657,377 Princess
May
33.2 Quartz carbonate vein
55049 636,737 7,657,494 Princess
May
0.303 Carbonated mafic

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Clancy Exploration Limited (ASX: CLY)

ASX / Media Announcement

Sample Easting

g North Prospect Au ppm Description 636,737 7,657,494 Princess 0.199 Quartz carbonate vein May

55050

Notes: All coordinates reported in MGA94‐Zone 50

APPENDIX 2: JORC Code, 2012 Edition‐ Section 1

Section 1 Sampling Techniques and Data

(Criteria in this section apply to all succeeding sections.)

Criteria JORC Code explanation Comments
Sampling
techniques
Nature and quality of sampling (eg cut channels, random
chips,
or
specific
specialised
industry
standard
measurement tools appropriate to the minerals under
investigation, such as down hole gamma sondes, or
handheld XRF instruments, etc). These examples should
not be taken as limiting the broad meaning of sampling.
Reconnaissance rock chip sampling (152 samples) was completed by De Grey Mining
Ltd in 2008.

Rock chip conducted by visual identification of prospective lithological and
gossanous units within the historical Pilbara Well Greenstone Belt. Location of
samples was determined using a handheld Garmin GPS unit with an accuracy of
+/‐5m

Rock samples (De Grey) were sent to UltraTrace in Perth, where they were dried,
crushed, pulverised and split to produce a sub–sample for Aqua Regia digestion
on a 50g sample with Atomic Absorption Spectroscopy undertaken to determine
gold content with a detection limit of 0.005ppm. All other elements (18 in total)
were read by inductively coupled plasma – optical emission spectroscopy
technique (ICP‐OES) (Ag, As, Ba, Bi, Hg, Li, Mo, Pt, Sb, Sn, U and W) with various
detection limits or inductively coupled plasma – mass spectroscopy (Cu, Fe, Mn,
Ni, Pb, and Zn).
Include reference to measures taken to ensure sample
representivity and the appropriate calibration of any
measurement tools or systems used.
Rock chip samples taken typically weigh in the range of 3 to 4kg. Representativeness
cannot be ascertained as it was not recorded.
Aspects of the determination of mineralisation that are
Material to the Public Report. In cases where ‘industry
standard’ work has been done this would be relatively
simple (eg ‘reverse circulation drilling was used to obtain
1 m samples from which 3 kg was pulverised to produce a
30 g charge for fire assay’). In other cases more
explanation may be required, such as where there is
coarse gold that has inherent sampling problems. Unusual
commodities or mineralisation types (eg submarine
nodules)maywarrant disclosure of detailed information.
A 3‐4kg rock chip sample was sampled and sent for analysis at Ultratrace laboratory in
Perth where the sample was dried, crushed, pulverised and split to produce a 50g sub
sample. The sub sample underwent Aqua Regia Digestion with Atomic Absorption
Spectroscopy for gold and Inductively Coupled Plasma‐Optical Emission Spectroscopy
for base metals.
Drilling
techniques
Drill type (eg core, reverse circulation, open‐hole
hammer, rotary air blast, auger, Bangka, sonic, etc) and
details (eg core diameter, triple or standard tube, depth
of diamond tails, face‐sampling bit or other type, whether
core is oriented and if so,bywhat method,etc).
No drilling conducted.
Drill
Sample
Recovery
Method of recording and assessing core and chip sample
recoveries and results assessed.
No drilling conducted.
Measures taken to maximise sample recovery and ensure
representative nature of the samples.
No drilling conducted.
Whether a relationship exists between sample recovery
and grade and whether sample bias may have occurred
due topreferential loss/gain of fine/coarse material.
No drilling conducted.
Logging Whether core and chip samples have been geologically
and geotechnically logged to a level of detail to support
appropriate Mineral Resource estimation, mining studies
and metallurgical studies.
No drilling conducted.
Whether logging is qualitative or quantitative in nature.
Core(or costean,channel,etc) photography.
Rock chip samples were visually logged and some photographed
The total length and percentage of the relevant
intersections logged.
No drilling conducted
Sub‐
sampling
If core, whether cut or sawn and whether quarter, half or
all core taken.
No diamond drilling completed

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Clancy Exploration Limited (ASX: CLY)

Criteria JORC Code explanation Comments
techniques
and sample
preparation
If non‐core, whether riffled, tube sampled, rotary split, etc
and whether sampled wet or dry.
3 to 4 kg rock chip sample was collected from the selected outcrops
For all sample types, the nature, quality and
appropriateness of the sample preparation techniques
Whole rock samples were submitted to UltraTrace for crushing, grinding and assaying
in accordance with industry best practices. No field preparation of samples was
conducted
Quality control procedures adopted for all sub‐sampling
stages to maximise representivityof samples.
No QC procedures are documented
Measures taken to ensure that the sampling is
representative of the in situ material collected, including
for instance results for field duplicate/second‐half
sampling.
No QAQC procedures are documented
Whether sample sizes are appropriate to the grain size of
the material beingsampled.
Sufficient sample mass was collected to provide a representative sample.
Quality of
assay data
and
laboratory
tests
The nature, quality and appropriateness of the assaying
and laboratory procedures used and whether the
technique is consideredpartial or total.
Samples were submitted to UltraTrace for sample preparation and analysis using aqua
regia digestion and read by graphite furnace for gold and ICP‐mass spectrometry or
optical emission spectrometryfor other elements
For geophysical tools, spectrometers, handheld XRF
instruments, etc, the parameters used in determining the
analysis including instrument make and model, reading
times, calibrations factors applied and their derivation,
etc.
No geophysical tools utilised.
Nature of quality control procedures adopted (eg
standards, blanks, duplicates, external laboratory checks)
and whether acceptable levels of accuracy (ie lack of bias)
andprecision have been established.
No QAQC samples reported
Verification
of sampling
and
assaying
The verification of significant intersections by either
independent or alternative company personnel.
No drilling completed.
The use of twinned holes. No drillingcompleted.
Documentation of primary data, data entry procedures,
data verification, data storage (physical and electronic)
protocols.
No documentation available with respect to capture of primary data. Data available
through WAMEX report system was captured into a validated GIS database.
Discuss anyadjustment to assaydata. No adjustments wereperformed to data.
Location of
Data Points
Accuracy and quality of surveys used to locate drill holes
(collar and down‐hole surveys), trenches, mine workings
and other locations used in Mineral Resource estimation.
Samples were located using a Garmin handheld GPS with an accuracy of +/‐ 5m (De
Grey).
Specification of thegrid system used. MGA94‐ Zone 50
Qualityand adequacyof topographic control. Topographic control usingGPS is more than adequate for rock chipsampling.
Data
spacing and
distribution
Data spacing for reporting of Exploration Results. Rock chip sampling was completed across areas of geological interest. Sampling was
not completed on a regulargrid.
Whether the data spacing and distribution is sufficient to
establish the degree of geological and grade continuity
appropriate for the Mineral Resource and Ore Reserve
estimationprocedure(s)and classifications applied.
Sampling reported is of reconnaissance nature and not for the purposes of the
delineation of a mineral resource.
Whether sample compositinghas been applied. No compositingapplied.
Orientation
of data in
relation to
geological
structure
Whether the orientation of sampling achieves unbiased
sampling of possible structures and the extent to which
this is known,consideringthe deposit type.
Sampling was selective to determine the tenor and nature of mineralisation.
If the relationship between the drilling orientation and the
orientation of key mineralised structures is considered to
have introduced a sampling bias, this should be assessed
and reported if material.
No drilling reported.
Sample
security
The measures taken to ensure sample security. No documentation exists with respect to sample security protocol.
Audits or
reviews
The results of any audits or reviews of sampling
techniques and data.
No audits or reviews have been conducted.

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Clancy Exploration Limited (ASX: CLY)

ASX / Media Announcement

JORC Code, 2012 Edition‐ Section 2

Section 2 Reporting of Exploration Results

(Criteria listed in the preceding section also apply to this section.)

Criteria JORC Code explanation Commentary
Mineral tenement and land
tenure status
Type, reference name/number, location and ownership
including agreements or material issues with third
parties such as joint ventures, partnerships, overriding
royalties, native title interests, historical sites, wilderness
or nationalpark and environmental settings.
The granted Exploration Licence E47/3566 has been acquired by Clancy
Exploration Ltd
The security of the tenure held at the time of reporting
along with any known impediments to obtaining a
licence to operate in the area.
The Exploration Licence is located wholly within the Yandeyarra
Aboriginal Reserve. Access permits and consent is required in order to
operate within the Exploration Licence.
Exploration Acknowledgment and appraisal of exploration by other
parties.
Exploration has been ongoing since 1998 through various parties: the
Farno group, Bullion, Chalice Gold Mines and De Grey Mining mainly
through option arrangements with the previous owner. The data
pertainingto these exploration activities ispresented in this report.
Geology Deposit type, geological setting and style of
mineralisation.
The Hong Kong Project is located along the southeastern margin of the
Pilbara Well Greenstone Belt. The northeasterly trending greenstone
belt is up to 8.6km wide and forms a northeast‐plunging synform over
a strike length of 40km. The PWGB has experienced multiple phases of
ductile deformation and metamorphism, and consists mainly of basalts
and ultramafic rocks, with silicified sedimentary rocks. Several chert
interbeds, and minor metamorphosed felsic volcanic and sedimentary
units occur within the mafic–ultramafic sequence.
Goldmineralisation parallels lithological contacts and foliation in
amphibolite host rocks located in the highly sheared margin to the Yule
Granitic Complex. Bedrock‐hosted gold was mined from metre‐scale,
foliation‐parallel quartz veins, however, vein widths can be as great 20
metres wide and strike northeast over several hundred metres. Gold is
hosted in quartz‐carbonate veins in carbonated mafic to ultramafic
rocks, and represent typical Archaean orogenic gold deposits. Gold is
most likely concentrated in shear zones and the faulted contacts
between units of contrasting competencies and lithology. Sericite and
carbonate alteration, with secondary malachite, chalcopyrite, and
sphalerite is often associated withgold.
Drill Hole Information A summary of all information material to the
understanding of the exploration results including a
tabulation of the following information for all Material
drill holes:
No drilling reported.
o easting and northing of the drill hole collar No drilling reported.
o elevation or RL (Reduced Level – elevation above sea
level in metres)of the drill hole collar
No drilling reported.
o dip and azimuth of the hole No drilling reported.
o down hole length and interception depth No drilling reported.
o hole length. No drilling reported.
If the exclusion of this information is justified on the
basis that the information is not Material and this
exclusion does not detract from the understanding of
the report, the Competent Person should clearly explain
why this is the case.
All available historical exploration information has been included in the
release. A more comprehensive evaluation of activities conducted
across the Project historically is underway.
Data Aggregation Methods In reporting Exploration Results, weighting averaging
techniques, maximum and/or minimum grade
truncations (eg cutting of high grades) and cut‐off grades
are usuallyMaterial and should be stated.
No modification of results was performed.
Where aggregate intercepts incorporate short lengths of
high grade results and longer lengths of low grade
results, the procedure used for such aggregation should
be stated and some typical examples of such
aggregations should be shown in detail.
No aggregation of data was conducted.
The assumptions used for any reporting of metal
equivalent values should be clearlystated.
No metal equivalents are reported.
Relationship between
mineralisation widths and
intercept lengths
These relationships are particularly important in the
reportingof Exploration Results.
No drilling reported.
If the geometry of the mineralisation with respect to the
drill hole angle is known,its nature should be reported.
No drilling reported.
If it is not known and only the down hole lengths are
reported, there should be a clear statement to this effect
(eg ‘down hole length, true width not known’).
No drilling reported.
Diagrams Appropriate maps and sections (with scales) and
tabulations of intercepts should be included for any
significant discovery being reported These should
include, but not be limited to a plan view of drill hole
collar locations and appropriate sectional views.
Plans of project geology, targets, historical workings have been
included in the body of this release.

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Clancy Exploration Limited (ASX: CLY)

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Criteria JORC Code explanation Commentary
Balanced Reporting Where comprehensive reporting of all Exploration
Results is not practicable, representative reporting of
both low and high grades and/or widths should be
practiced to avoid misleading reporting of Exploration
Results.
All results including those with no significant results have been
included in the release.
Other substantive
exploration data
Other exploration data, if meaningful and material,
should be reported including (but not limited to):
geological observations; geophysical survey results;
geochemical survey results; bulk samples – size and
method of treatment; metallurgical test results; bulk
density, groundwater, geotechnical and rock
characteristics; potential deleterious or contaminating
substances.
All available information has been included in the release.
Further Work The nature and scale of planned further work (eg tests
for lateral extensions or depth extensions or large‐scale
step‐out drilling).
An extensive review of the open file information relating to the Project
will be completed in conjunction with a detailed geological mapping
program targeting the contact between the base of the Lower
Fortescue Groupand underlyingArchaean lithologies.
Diagrams clearly highlighting the areas of possible
extensions, including the main geological interpretations
and future drilling areas, provided this information is not
commerciallysensitive.
Further releases will be made to market upon completion of further
exploration planning.

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